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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Arctic region
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Asia
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Primary terms
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Highland region Scotland
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metamorphic rocks
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upper Precambrian
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Laxfordian
Seawater signatures in the supracrustal Lewisian Complex, Scotland
A regional explanation for Laxfordian tectonic evolution and its implications for the Lewisian terrane model
The nature and age of Mesoproterozoic strike-slip faulting based on Re–Os geochronology of syntectonic copper mineralization, Assynt Terrane, NW Scotland
Dykes as physical buffers to metamorphic overprinting: an example from the Archaean–Palaeoproterozoic Lewisian Gneiss Complex of NW Scotland
Evidence for pre-Caledonian discontinuities in the Achnashellach Culmination, Moine Thrust Zone: the importance of a pre-thrust template in influencing fold-and-thrust belt development
The Palaeoproterozoic anatomy of the Lewisian Complex, NW Scotland: evidence for two ‘Laxfordian’ tectonothermal cycles
Lewisian Complex of Strath Dionard–Rhiconich and its significance in the early history of the NW Highlands of Scotland
The South Barra shear zone: A composite Inverian–Laxfordian shear zone and possible Terrane boundary in the Lewisian gneiss complex of the Isle of Barra, NW Scotland
Structure and evolution of the Lewisian Gairloch shear zone: variable movement directions in a strike-slip regime
The Lewisian terrane model: a review
Discussion on a terrane-based nomenclature for the Lewisian Gneiss Complex of NW Scotland Journal , Vol. 162, 2005, pp. 175–186
A re-evaluation of a Laxfordian terrane boundary in the Lewisian Complex of South Harris, NW Scotland
The initiation and early tectonic significance of the Outer Hebrides Fault Zone, Scotland
Abstract This Memoir presents a detailed account of one of the most critical and interesting parts of the Lewisian complex of NW Scotland; a detached fragment of a supercontinent made up of Laurentia, Siberia and Baltica, which existed at the end of the early Proterozoic period. The Gairloch area, together with neighbouring Loch Maree, is the only part of the mainland Lewisian outcrop where Palaeoproterozoic supracrustal rocks (the Loch Maree Group] and their relationships to the Archaean basement can be studied, and has been the subject of a considerable amount of research, spanning a period of more than forty years. The Loch Maree Group represents an amalgamation of oceanic, trench, and arc assemblages with continental basement, and forms part of a Palaeoproterozoic collisional orogen stretching from Labrador through South Greenland to Scandinavia. The author is Emeritus Professor of Tectonic Geology at Keele University, England, and has studied the structural geology of Precambrian terrains in many parts of the world. He has mapped the area covered by the Memoir in detail, at a scale of 1:10 000, and has an intimate knowledge of the geology, acquired over many years.